Journalartikel

Jahr der Veröffentlichung: 1986

Seiten: 327-336

Zeitschrift: Archives of Agronomy and Soil Science

Bandnummer: 30

Heftnummer: 6

ISSN: 0365-0340

Verlag: Taylor and Francis Group

Abstract: 
Using an analytical solution of the non-steady-state internal drainage equation according to GARDNER, the calculation of mean diffusivity according to CRANK is an iterative scheme and the .THETA.(h.sigma.) and D(.THETA.) functions according to VAN GENUCHTEN, the internal drainage of 17 soil profiles of different texture was calculated for three groundwater table depths. The results show the time-dependent discharge and are used for discussing the conventional terms field capacity and moisture equivalent.

Harvard-Zitierstil: BOHNE, K. and WEGMANN, C. (1986) INTERPRETATION OF FIELD-CAPACITY AND MOISTURE EQUIVALENT ON THE BASIS OF THE THEORY OF FLOW, Archives of Agronomy and Soil Science, 30(6), pp. 327-336

APA-Zitierstil: BOHNE, K., & WEGMANN, C. (1986). INTERPRETATION OF FIELD-CAPACITY AND MOISTURE EQUIVALENT ON THE BASIS OF THE THEORY OF FLOW. Archives of Agronomy and Soil Science. 30(6), 327-336.